U.S. Department of Energy Office of Biological and Environmental Research

PI-Submitted Research Highlights for
Subsurface Biogeochemical Research Program

Potential for Reoxidation of Iron-Chromium Precipitates by Manganese Oxide

Elizabeth C. Butler
University of Oklahoma


Abiotic reduction of Cr(VI) by FeS and reduced nontronite led to precipitates that released significant Cr(VI) when exposed to birnessite.  Figure reproduced from Environ. Sci.: Processes Impacts 17 (2016), 1930–1940 (DOI: 10.1039/C5EM00286A) with permission from the Royal Society of Chemistry.

Reductive immobilization of hexavalent chromium (Cr(VI)), often forming Fe-Cr precipitates, is a frequent remediation alternative, yet the relationship between the conditions of precipitate formation, the structural and chemical properties of the precipitates, and the rate and extent of precipitate oxidation by Mn oxides is needed.  This study provided a systematic investigation of the rates of Cr(VI) reduction by both abiotic minerals and a chromium reducing bacterium, the properties of the resulting Fe-Cr precipitates, and the susceptibility for reoxidation and remobilization of Cr(VI) upon precipitate exposure to the manganese oxide birnessite. 

The properties of the resulting Fe-Cr solids and their behavior upon exposure to birnessite differed significantly.  In microcosms where Cr(VI) was reduced by Desulfovibrio vulgaris strain RCH1, and where hematite or Al-goethite were present as iron sources, there was significant initial loss of Cr(VI) in a pattern consistent with adsorption, and significant Cr(VI) was found in the resulting solids.  The solid formed when Cr(VI) was reduced by FeS contained a high proportion of Cr(III) and was poorly crystalline.  Reaction between birnessite and the abiotically formed Cr(III) solids led to production of significant dissolved Cr(VI) compared to the no-birnessite controls.  This pattern was not observed in the solids generated by microbial Cr(VI) reduction, and could be due to re-reduction of any Cr(VI) generated upon oxidation by birnessite via active bacteria or microbial enzymes. 

The results of this study suggest that Fe-Cr precipitates formed in groundwater remediation may remain stable only in the presence of active anaerobic microbial reduction.  If exposed to environmentally common Mn oxides such as birnessite in the absence of microbial activity, there is the potential for rapid (re)formation of dissolved Cr(VI) above regulatory levels.


Butler, E. C., Chen, L., Hansel, C. M., Krumholz, L. R., Elwood Madden, A. S., Lan, Y. (2015), Biological versus mineralogical chromium reduction: Potential for reoxidation by manganese oxide, Environ. Sci.: Processes Impacts 17, 1930–1940, DOI: 10.1039/C5EM00286A.

Additional information

Co-Investigators: Lee Krumholz, University of Oklahoma; Andrew Elwood Madden, University of Oklahoma; Colleen Hansel, Woods Hole Oceanographic Institution.

Funding for this work was provided by the U. S. Department of Energy Subsurface Biogeochemical Research Program (grant DE-SC0006902).  Part of this research was conducted at the Stanford Synchrotron Radiation Lightsource. Use of the Stanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, is supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences under Contract No. DE-AC02-76SF00515.  

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